The COSC-1 borehole located in the Lower Seve nappe of the Central Scandinavian Caledonides is intended to study the tectonic evolution of the Paleozoic orogen. The drilling project reached a depth of 2495.8m and obtained samples from different lithologal units of mica schist, amphibolite, gneiss, and mylonitic gneisses.     To test if the samples are suitable for paleomagnetism, laboratory measurements of natural remanent magnetism are performed on sub-samples of the COSC-1 drill core in the paleomagnetic laboratory with alternating field demagnetization, IRM acquisition as well as the temperature dependence of susceptibility measurements. Important properties of the samples such as coercivity, Curie temperature, inclination, and declination are determined with the measurements.     Most of the samples carry a remanent magnetization that can be readily demagnetized with alternating field demagnetization up to 100 mT. Some of the samples may be suitable for paleomagnetism, with the major ferromagnetic mineral compositions of magnetite, hematite, and FeTi oxides. However, low coercivities and median destructive fields suggest that the magnetite-bearing samples will be prone to remagnetization, making them more challenging to use in terms of retrieving a primary magnetization originating from the Caledonian orogeny. The thermomagnetic results of some samples reflect the metamorphic conditions experienced by the rocks and the mineral assemblage changed irreversibly during step-wise heating experiments. These results can possibly be used as an indicator for the metamorphic temperature experienced by the different lithologal units. Although further measurements are needed to get a clearer understanding of the suitability of the COSC-1 sample for paleomagnetic reconstructions (including thermal demagnetization experiments), this thesis indicates that the COSC-1 rocks contain interesting paleo- and rock magnetic features that are worth further study.

京都大学 / 0048 / 新制・課程博士 / 博士(医学) / 甲第20564号 / 医博第4249号 / 新制||医||1022(附属図書館) / 京都大学大学院医学研究科医学専攻 / (主査)教授 増永 慎一郎, 教授 妹尾 浩, 教授 鈴木 実 / 学位規則第4条第1項該当 / Doctor of Medical Science / Kyoto University / DFAM

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В работе изучается динамическая восприимчивость феррожидкости, которая моделируется системой взаимодействующих подвижных магнитных частиц. Предполагается, что система находится в постоянном и переменном магнитном полях, направленных параллельно друг другу. / In this work, we study the dynamic susceptibility of a ferrofluid, which is modeled by an system of interacting moving magnetic particles. It is assumed that the system is in a constant and an alternating magnetic field, directed parallel to each other.

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Ever since the discovery of the giant magnetocaloric effect (GMCE) in the Gd5(Si,Ge)4 phases, magnetic cooling has gained significant interest because of its potential environmental benefits and increased efficiency compared to vapour-based refrigeration. This current work is focused on one of the most promising GMCE systems, the (Mn,Fe)2(Si,P) materials. An alternative synthetic route has been explored for the Mn2-xFexSi0.5P0.5 and MnFeSiyP1-y series which is capable of producing phase-pure samples. The new preparation technique eliminates common impurities that arise from established methods thus providing a more accurate description of the structural and physical properties. The low cost, non-toxicity, abundance of starting materials and easy tuning of the magnetic properties make these materials desirable for potential applications. Phase-pure magnetocaloric Mn2-xFexSi0.5P0.5 materials (x = 0.6, 0.7, 0.8, 0.9) were synthesized through arc-melting followed by high temperature sintering. Structural features of samples with x = 0.6, 0.9 were studied through temperature dependent synchrotron powder x-ray diffraction. Magnetic measurements established the Curie temperature, thermal hysteresis, and magnetic entropy change of this system. According to the diffraction and magnetization data, all of the samples were shown to have a first-order magnetostructural transition which becomes less pronounced for Mn-richer samples. The MnFeSixP1-x phases (x = 0.30, 0.35, 0.40, 0.48, 0.52, 0.54, 0.56) have also been synthesized by the same method. For the first time, single crystals of x = 0.30, 0.40 were successfully grown. Variable temperature x-ray diffraction experiments for x = 0.30 were completed which show the structural changes across the phase transition. This structural data was complemented with magnetization data providing Curie temperatures and thermal hysteresis. / Thesis / Master of Science (MSc)

Approximately 23% of Canadians over the age of 65 are considered frail, with that number predicted to increase up to 40% for the population over the age of 85. Frailty is a geriatric syndrome defined by the natural decline in muscle mass and function caused by the natural aging process. When developing to an excessive degree, frailty may present as a disease state, which is recognized as sarcopenia. The exact definition of sarcopenia relies on the presence of low muscle mass, strength, and/or function, but quantitative cut-off values are still a topic of debate. Understanding how biomarkers measured via diagnostic imaging such as magnetic resonance imaging (MRI) and dual-energy x-ray absorptiometry (DXA) describe skeletal muscle can allow doctors to develop a profile of sarcopenia and define predictors to aide in preventative therapy. 4 male and 9 female (mean age = 78 ± 6.5 years) participants from a frailty study underwent full-body DXA and had their dominant thigh scanned using a 3.0T MRI. DXA-derived appendicular lean mass (ALM) and MRI-derived cross-sectional area (CSA), fat fraction (FF), T2 relaxation (T2), magnetization transfer ratio (MTR), fractional anisotropy (FA) and mean diffusivity (MD) from 4 muscle groups at the mid-thigh were defined as muscle biomarkers. Pearson's correlation was calculated to identify relationships between biomarkers and a Wilcoxon rank-sum test was performed to assess the agreement of low-muscle mass characterization between ALM normalized by height (ALMI), ALM normalized by BMI (ALM/BMI), and the gold standard MRI cross-sectional area. Strong positive correlations between muscle quantity biomarkers such as ALMI and CSA were recognized within the quadriceps (p=0.0095), adductors (p=0.035), and sartorius (p=0.00065) muscles while muscle quality biomarkers such as FF and T2 showed significant positive correlation within the quadriceps (p=3.58*10^-5) and the hamstring (p=0.0042) muscles. Finally, ALM/BMI displayed a much stronger agreement in muscle mass quantification with the gold-standard of MRI-CSA over the more commonly researched ALMI from DXA. The main purpose of this study was to collate a vast array of skeletal muscle biomarkers obtained using DXA and MRI on a frail population, and show that significant correlations can be recognized from a single MRI-slice located at the mid-thigh. Additionally, this study recognized the potential of ALM/BMI as the DXA-derived biomarker of choice in muscle mass assessment of frailty. / Thesis / Master of Applied Science (MASc) / A person is diagnosed with sarcopenia when they present symptoms of low muscle mass, strength, and/or function. Defining these three criteria with objective measures has been long debated by researchers and clinicians alike. By understanding how different properties, or biomarkers, of skeletal muscle relate to one another and change as a person becomes more frail, we hope to better understand sarcopenia and identify the best measures to classify someone as sarcopenic. Being able to accurately diagnose someone as sarcopenic early allows for more effective treatment of this muscle disease. In this study, non-invasive magnetic resonance imaging (MRI) and dual energy x-ray absorptiometry (DXA) were used to measure many different biomarkers of skeletal muscle at the mid-thigh. Through characterizing these measures of muscle quality and quantity between different imaging techniques this study aimed to recognize which imaging techniques, and more specifically biomarkers, can best distinguish between a person who is sarcopenic and one who is non-sarcopenic.